Evidence of a strong coupling between root exudation, C and N availability, and stimulated SOM decomposition caused by rhizosphere priming effects
(2012) In Ecology and Evolution 2(8). p.1843-1852- Abstract
- Increased temperatures and concomitant changes in vegetation patterns are expected to dramatically alter the functioning of northern ecosystems over the next few decades. Predicting the ecosystem response to such a shift in climate and vegetation is complicated by the lack of knowledge about the links between aboveground biota and belowground process rates. Current models suggest that increasing temperatures and rising concentrations of atmospheric CO2 will be partly mitigated by elevated C sequestration in plant biomass and soil. However, empirical evidence does not always support this assumption, as elevated temperature and CO2 concentrations also accelerate the belowground C flux, in many cases extending to increased decomposition of... (More)
- Increased temperatures and concomitant changes in vegetation patterns are expected to dramatically alter the functioning of northern ecosystems over the next few decades. Predicting the ecosystem response to such a shift in climate and vegetation is complicated by the lack of knowledge about the links between aboveground biota and belowground process rates. Current models suggest that increasing temperatures and rising concentrations of atmospheric CO2 will be partly mitigated by elevated C sequestration in plant biomass and soil. However, empirical evidence does not always support this assumption, as elevated temperature and CO2 concentrations also accelerate the belowground C flux, in many cases extending to increased decomposition of soil organic matter (SOM) and ultimately resulting in decreased soil C stocks. The mechanism behind the increase has remained largely unknown, but it has been suggested that priming might be the causative agent. Here, we provide quantitative evidence of a strong coupling between root exudation, SOM decomposition, and release of plant available N caused by rhizosphere priming effects. As plants tend to increase belowground C allocation with increased temperatures and CO2 concentrations, priming effects need to be considered in our long-term analysis of soil C budgets in a changing environment. The extent of priming seems to be intimately linked to resource availability, as shifts in the stoichiometric nutrient demands of plants and microorganisms will lead to either cooperation (resulting in priming) or competition (no priming will occur). The findings lead us on the way to resolve the varying response of primary production, SOM decomposition, and release of plant available N to elevated temperatures, CO2 concentrations, and N availability. (Less)
Please use this url to cite or link to this publication:
https://lup.lub.lu.se/record/3371977
- author
- Bengtson, Per LU ; Barker, Jason and Grayston, Sue J.
- organization
- publishing date
- 2012
- type
- Contribution to journal
- publication status
- published
- subject
- keywords
- Carbon sequestration, coupled biogeochemical cycles, elevated CO2, global warming, microbial C assimilation, nitrogen mineralization, plant-microbial feedbacks, soil respiration
- in
- Ecology and Evolution
- volume
- 2
- issue
- 8
- pages
- 1843 - 1852
- publisher
- Wiley-Blackwell
- external identifiers
-
- wos:000312448700007
- scopus:84876487095
- pmid:22957187
- ISSN
- 2045-7758
- DOI
- 10.1002/ece3.311
- language
- English
- LU publication?
- yes
- id
- 82dbdaa6-b8b0-4c01-9b26-5311bc16db6f (old id 3371977)
- date added to LUP
- 2016-04-01 15:04:23
- date last changed
- 2022-04-22 06:42:13
@article{82dbdaa6-b8b0-4c01-9b26-5311bc16db6f,
abstract = {{Increased temperatures and concomitant changes in vegetation patterns are expected to dramatically alter the functioning of northern ecosystems over the next few decades. Predicting the ecosystem response to such a shift in climate and vegetation is complicated by the lack of knowledge about the links between aboveground biota and belowground process rates. Current models suggest that increasing temperatures and rising concentrations of atmospheric CO2 will be partly mitigated by elevated C sequestration in plant biomass and soil. However, empirical evidence does not always support this assumption, as elevated temperature and CO2 concentrations also accelerate the belowground C flux, in many cases extending to increased decomposition of soil organic matter (SOM) and ultimately resulting in decreased soil C stocks. The mechanism behind the increase has remained largely unknown, but it has been suggested that priming might be the causative agent. Here, we provide quantitative evidence of a strong coupling between root exudation, SOM decomposition, and release of plant available N caused by rhizosphere priming effects. As plants tend to increase belowground C allocation with increased temperatures and CO2 concentrations, priming effects need to be considered in our long-term analysis of soil C budgets in a changing environment. The extent of priming seems to be intimately linked to resource availability, as shifts in the stoichiometric nutrient demands of plants and microorganisms will lead to either cooperation (resulting in priming) or competition (no priming will occur). The findings lead us on the way to resolve the varying response of primary production, SOM decomposition, and release of plant available N to elevated temperatures, CO2 concentrations, and N availability.}},
author = {{Bengtson, Per and Barker, Jason and Grayston, Sue J.}},
issn = {{2045-7758}},
keywords = {{Carbon sequestration; coupled biogeochemical cycles; elevated CO2; global warming; microbial C assimilation; nitrogen mineralization; plant-microbial feedbacks; soil respiration}},
language = {{eng}},
number = {{8}},
pages = {{1843--1852}},
publisher = {{Wiley-Blackwell}},
series = {{Ecology and Evolution}},
title = {{Evidence of a strong coupling between root exudation, C and N availability, and stimulated SOM decomposition caused by rhizosphere priming effects}},
url = {{http://dx.doi.org/10.1002/ece3.311}},
doi = {{10.1002/ece3.311}},
volume = {{2}},
year = {{2012}},
}